dor_id: 4133243

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

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270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/147/141

100.1.#.a: Ávila-carrera, Rafael; Rodríguez-castellanos, Alejandro; Valle-molina, Celestino; González-flores, Ernesto; Sánchez-sesma, Francisco José; Luzón, Francisco

524.#.#.a: Ávila-carrera, Rafael, et al. (2016). Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks. Geofísica Internacional; Vol. 55 Núm. 4: Octubre 1, 2016; 275-291. Recuperado de https://repositorio.unam.mx/contenidos/4133243

245.1.0.a: Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2016

264.#.1.c: 2016-10-01

653.#.#.a: Modelo de propagación de onda; grietas cercanas a la superficie; respuesta sísmica; wave propagation model; near surface cracks; seismic response

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/147

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/147

041.#.7.h: spa

520.3.#.a: Scattering and diffraction of P and SV waves caused by parallel oriented cracks located near to a free surface are investigated in this work. The Indirect Boundary Element Method (IBEM) was applied for studying the wave propagation phenomena in a half-plane model that contain the cracks. Various incidence angles of P and SV waves are considered. Sometime before it has been reported that a near free-surface crack generates scattered surface waves whose amplitude spectra show conspicuous resonance peaks. Such effect has been attributed to local resonances originated in a virtual layer between the shallowest crack and the free surface. For our case of two parallel crack system, where cracks are located at different depths, the amplitude spectra show additional peaks, which can be associated with the presence of the second crack. Given similar sizes between these two cracks, the characteristic resonance frequency observed at the free surface corresponds mainly to the equivalent layer formed by the shallowest crack and the free surface. However, when the deepest crack becomes sufficiently large with respect to the shallow crack, two resonance characteristic frequency peaks appear in the measured spectra at the free surface. Some examples including a three crack system are also illustrated in our work. The identification and characterization of the seismic response for the scattered field generated by the second and third crack has been an intricate task and, the time domain interpretation of traces becomes quite complicated. The results in this paper have been validated against some other reported from classic papers. In order to show the seismic response and multiple scattering effects due to the presence of systems of cracks, calculations in frequency and time domain are provided.doi: https://doi.org/10.22201/igeof.00167169p.2016.55.4.1729

773.1.#.t: Geofísica Internacional; Vol. 55 Núm. 4: Octubre 1, 2016; 275-291

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 275-291

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2016.55.4.1729

handle: 00ef357ed7f1f0c9

harvesting_date: 2023-06-20 16:00:00.0

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file_modification_date: 2022-04-01 20:46:43.0

file_creator: Rafael Ávila-Carrera

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245.1.0.b: Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks

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Artículo

Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks

Ávila-carrera, Rafael; Rodríguez-castellanos, Alejandro; Valle-molina, Celestino; González-flores, Ernesto; Sánchez-sesma, Francisco José; Luzón, Francisco

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Ávila-carrera, Rafael, et al. (2016). Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks. Geofísica Internacional; Vol. 55 Núm. 4: Octubre 1, 2016; 275-291. Recuperado de https://repositorio.unam.mx/contenidos/4133243

Descripción del recurso

Autor(es)
Ávila-carrera, Rafael; Rodríguez-castellanos, Alejandro; Valle-molina, Celestino; González-flores, Ernesto; Sánchez-sesma, Francisco José; Luzón, Francisco
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks
Fecha
2016-10-01
Resumen
Scattering and diffraction of P and SV waves caused by parallel oriented cracks located near to a free surface are investigated in this work. The Indirect Boundary Element Method (IBEM) was applied for studying the wave propagation phenomena in a half-plane model that contain the cracks. Various incidence angles of P and SV waves are considered. Sometime before it has been reported that a near free-surface crack generates scattered surface waves whose amplitude spectra show conspicuous resonance peaks. Such effect has been attributed to local resonances originated in a virtual layer between the shallowest crack and the free surface. For our case of two parallel crack system, where cracks are located at different depths, the amplitude spectra show additional peaks, which can be associated with the presence of the second crack. Given similar sizes between these two cracks, the characteristic resonance frequency observed at the free surface corresponds mainly to the equivalent layer formed by the shallowest crack and the free surface. However, when the deepest crack becomes sufficiently large with respect to the shallow crack, two resonance characteristic frequency peaks appear in the measured spectra at the free surface. Some examples including a three crack system are also illustrated in our work. The identification and characterization of the seismic response for the scattered field generated by the second and third crack has been an intricate task and, the time domain interpretation of traces becomes quite complicated. The results in this paper have been validated against some other reported from classic papers. In order to show the seismic response and multiple scattering effects due to the presence of systems of cracks, calculations in frequency and time domain are provided.doi: https://doi.org/10.22201/igeof.00167169p.2016.55.4.1729
Tema
Modelo de propagación de onda; grietas cercanas a la superficie; respuesta sísmica; wave propagation model; near surface cracks; seismic response
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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